Abstract

The following paper summarizes the history of Gelnica, Smolník and Rožňava gold, silver, copper and iron orefields in Eastern Slovakia, which have been mined since the Medieval ages by of Slovak and German miners. In Gelnica, where mining operations date back to the XIIth century, massive quartz-sideritechalcopyrite veins with Fe-dolomite, pyrite and tetrahedrite (with silver) cut Lower Devonian phyllites and porphyroids. In Smolník, where copper mining has commenced in the first half of the XIIIth century followed by gold, then silver and iron ore exploitation, 10-11 pyrite-chalcopyrite ore horizons are hosted in Silurian phyllites. In Rožňava mining operations for iron, silver, gold and copper ores have been known since the XIIIth century and have lasted until 1992. Over 40 ore veins discovered in this field contain mostly siderite although quartz-siderite-sulphide paragenesis with Ag-bearing tetrahedrite was also observed. In all three mining districts there are numerous objects of mining heritage and other valuable historical monuments, reflecting the wealth of old Slovak mining towns.

Highlights

  • The Faculty BERG of the Technical University in Kosice, Slovakia organized a specialized meeting in order to follow the steps of Slovak and German miners in the historical ore mining districts of Gelnica, Smolník and Rožňava

  • On the day the program included visits to the sites of common history of Slovak and German miners working in Gelnica, Smolník and Rožňava districts (Fig. 3b)

  • The Hungarian royal decree issued in the year 1323 imposed a tax on gold mined in Rožňava

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Summary

Introduction

The Faculty BERG of the Technical University in Kosice, Slovakia organized a specialized meeting in order to follow the steps of Slovak and German miners in the historical ore mining districts of Gelnica, Smolník and Rožňava. Geotouristic excursion to selected historical mining sites is disseminated or massive chalcopyrite with some pyrite and tetrahedrite, the latter containing 0.4 wt% Ag, up to 12.6 wt.% Hg, 0.9-7.6 wt.% Fe and 1.1-5.3 wt.% Zn (Pauliš and Duda, 2002). Another important ore vein zone was located in the vicinity of Žakarovce. The ore graded 32-35 vol.% Fe, 0.1-0.2 vol.% Cu and 8-12 vol.% SiO2

Geological setting
The history of the Upper Ugrian mining towns
Conclusions
Budowa geologiczna
Historia miast górniczych na obszarze Górnych Węgier
Full Text
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